Structure of high elevation forests in Katunsky Range (the Altai Mountains)

Svetlana Nikolaeva, D. Savchuk, Aleksandr Kuznecov, E. Filimonova
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Abstract

High elevation forests are both a good natural object for studying the forest dynamics and a sensitive indicator of the impact of various external factors on them. These forests on the Katunsky Range of the Altai Mountains have been studied extremely poorly. The purpose of the work is to describe the size and age structure of tree stands of forest communities and to reveal the effect of environmental factors on them in the upper part of the forest belt of the Katunsky Range (the Altai Mountains) using the Akkem glacial basin as an example. Six sample areas of 0.05-0.12 ha were used at two altitude levels (2065-2080 and 2220-2240 m a.s.l.). A total of 232 adult trees and 209 saplings and seedlings were examined, aged 86 and 180, respectively. The size and age structure of the forest stand and saplings and seedlings has been established. Three main generations of trees that established on the valley slopes have been identified in the forest stand (the first generation is trees of 530-580 years old, the second is the trees of 270-410 years old, and the third is trees of 30-120 years old) and one additional generation (130-170 years old). They established at the end of the Medieval warming (XV-XVI centuries), during the Little Ice Age (XVII-mid-XIX centuries), and during the warming which began in the mid-XIX centuries. Factors have been identified that limit the spread and the structure of the high elevation forests: geomorphological, wildfires, logging.
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卡图恩斯基山脉(阿尔泰山)高海拔森林的结构
高海拔森林既是研究森林动态的良好自然对象,也是各种外部因素对其影响的敏感指标。人们对阿尔泰山卡屯斯基山脉的这些森林研究极少。这项工作的目的是以阿克坎冰川盆地为例,描述卡屯斯基山脉(阿尔泰山脉)森林带上部森林群落林木的大小和年龄结构,并揭示环境因素对它们的影响。在两个海拔高度(海拔 2065-2080 米和海拔 2220-2240 米)使用了六个面积为 0.05-0.12 公顷的样本区域。共考察了 232 株成年树、209 株树苗和幼苗,树龄分别为 86 年和 180 年。林分、树苗和幼苗的大小和年龄结构已经确定。在林分中发现,在山谷斜坡上生长的树木主要有三代(第一代为树龄 530-580 年的树木,第二代为树龄 270-410 年的树木,第三代为树龄 30-120 年的树木)和另外一代(树龄 130-170 年)。它们分别出现在中世纪气候变暖末期(XV-XVI 世纪)、小冰河时期(XVII-XIX 世纪中期)和 XIX 世纪中期开始的气候变暖时期。限制高海拔森林蔓延和结构的因素已经确定:地貌、野火、伐木。
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